Microbial Nitrogen Cycling Processes in a Sulfidic Coastal Marsh

Abstract

Sulfide distribution is a key controller of vegetation zonation in coastal ecosystems, but data are limited regarding its impact on the spatial distribution of important N cycling processes. We assessed vegetation distribution and density and, mineral N pool sizes, composition and transformations in a sulfidic coastal marsh in relation to distance from sulfur springs. We observed strong relationships between vegetation attributes (species and density) and mineral N status with greater total inorganic N, NO₃⁻ and denitrification enzyme activity (DEA) in sediment samples from areas populated by Crithmum maritimum (mid-way between S springs and sea shore) than in sediments from areas colonized by either Agropyron repens (closest to the S springs) or mangrove (Rhizophora mangleL., farthest from the springs). Our data also suggest close links between N cycling and SO₄⁻² reduction. The latter resulted in net release of NH₄⁺ ranging from 0.9 mg N kg⁻¹ in the low density C. maritimum to 3.2 mg N kg⁻¹ in the high-density A. repens, during a 3-day incubation. We also tested for microbial adaptation to long-term high sulfide exposure by measuring DEA using the C₂H₂ block method (which has been found to be strongly affected by the presence of sulfide) and amendment of marsh sediment samples with NaMoO₄ to suppress reduced S production. In sediments extracted from sites near the sulfur springs (A. repens and C. maritimum), the C₂H₂ blockage assay yielded similar results without and with NaMoO₄ addition. However, in samples from a mangrove located further downstream from the springs, DEA was substantially lower (2.3 vs. 6.8 mg N₂O-N kg⁻¹ sediment d⁻¹) when production of reduced S was not inhibited by NaMoO₄. These results suggest that denitrifying microbes in the high sulfide areas may have adapted to the presence of sulfide, allowing for high rates of N and S cycling to occur simultaneously in these marshes.